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Książki na temat „Variability of rainfall”

Autor: Grafiati

Data publikacji: 2 czerwca 2025

Data aktualizacji: 31 lipca 2025

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1

Nicholson, Sharon E. Atlas of African rainfall and its interannual variability. Florida State University, Department of Meteorology, 1988.

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Doi, Ram. Analysis of rainfall variability and drought occurrences in Rajasthan. Department of Geography, University of Reading, 1993.

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Doi, Ram. Analysis of rainfall variability and drought occurences in Rajasthan. University of Reading Department of Geography, 1993.

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Hermance, John F. Historical Variability of Rainfall in the African East Sahel of Sudan. Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-00575-1.

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Kim, Cornelis Pieter. The water budget of heterogeneous areas: Impact of soil and rainfall variability. [s.n.], 1995.

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Kulkarni, Ashwini. Examining Indian monsoon variability in coupled climate model simulations and projections. Indian Institute of Tropical Meteorology, 2010.

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Feddema, Johannes J. Evaluation of terrestrial climate variability using a moisture index. C.W. Thornthwaite Associates, Laboratory of Climatology ; Newark, Del., 1994.

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8

Mastura, Bte Mahmud. Mechanisms of winter monsoon rainfall variability across the eastern coast of peninsular Malaysia. University of Birmingham, 1991.

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9

Eric, Servat, African Association of Hydrology, and International Association of Hydrological Sciences., eds. Water resources variability in Africa during the XXth century =: Variabilité des ressources en eau en Afrique au XXème siècle : proceedings of the international conference "Water Resources Variability in Africa during the XXth century" held at Abidjan, 16-19 November, 1998. International Association of Hydrological Sciences, 1998.

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10

Morris, Susan E. Variability in storm rainfall over an upland catchment and its implications for storm runoff. The Polytechnic, 1989.

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11

Hulme, M. The tropical easterly jet and Sudan rainfall 2: Inter- and intra-annual variability during 1968-85. University of Salford Department of Geography, 1988.

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12

Groen, Maria Margaretha de. Modelling interception and transpiration at monthly time steps: Introducing daily variability through Markov chains. Swets & Zeitlinger, 2002.

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13

Jordan, Phillip William. Effect on flood modelling of rainfall variability and radar rainfall measurement error. 2000.

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14

Bandyopadhyay, Sushenjit, and Emmanuel koufias. Rainfall Variability, Occupational Choice, and Welfare in Rural Bangladesh. The World Bank, 2012. http://dx.doi.org/10.1596/1813-9450-6134.

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15

STUDIES OF RAINFALL AND NDVI VARIABILITY OVER SELECTED REGION OF SOUTHERN ETHIOPIA: Correlation between rainfall and NDVI. Mekonnen Daba, 2012.

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Seasonal Climatology, Variability, Characteristics, and Prediction of the Caribbean Rainfall Cycle. [publisher not identified], 2021.

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17

Hermance, John F. Historical Variability of Rainfall in the African East Sahel of Sudan: Implications for Development. Springer London, Limited, 2013.

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18

Hermance, John F. Historical Variability of Rainfall in the African East Sahel of Sudan: Implications for Development. Springer, 2013.

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19

STUDIES OF RAINFALL AND NDVI VARIABILITY OVER SELECTED REGION OF SOUTHERN ETHIOPIA. Mekonnen Daba, 2012.

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20

Les gradients climatiques en Tunisie: Application à la température et à la pluie. Publications de la Faculté des lettres de la Manouba, 2000.

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21

Kucharski, Fred, and Muhammad Adnan Abid. Interannual Variability of the Indian Monsoon and Its Link to ENSO. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.615.

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The interannual variability of Indian summer monsoon is probably one of the most intensively studied phenomena in the research area of climate variability. This is because even relatively small variations of about 10% to 20% from the mean rainfall may have dramatic consequences for regional agricultural production. Forecasting such variations months in advance could help agricultural planning substantially. Unfortunately, a perfect forecast of Indian monsoon variations, like any other regional climate variations, is impossible in a long-term prediction (that is, more than 2 weeks or so in adva

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22

Nash, David. Changes in Precipitation Over Southern Africa During Recent Centuries. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.539.

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Precipitation levels in southern Africa exhibit a marked east–west gradient and are characterized by strong seasonality and high interannual variability. Much of the mainland south of 15°S exhibits a semiarid to dry subhumid climate. More than 66 percent of rainfall in the extreme southwest of the subcontinent occurs between April and September. Rainfall in this region—termed the winter rainfall zone (WRZ)—is most commonly associated with the passage of midlatitude frontal systems embedded in the austral westerlies. In contrast, more than 66 percent of mean annual precipitation over much of th

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23

Hughes, Denis, Jean-Marie Fritsch, Mike Hulme, and Eric Servat. Series of Proceedings and Reports: Water Resources Variability in Africa During the XXth Century: Proceedings of the Abidjan 1998 Conference Held at Abidjan, ... 1998 (Series of Proceedings and Reports). IAHS Press, 1998.

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24

Norrgård, Stefan. Changes in Precipitation Over West Africa During Recent Centuries. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.536.

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Water, not temperature, governs life in West Africa, and the region is both temporally and spatially greatly affected by rainfall variability. Recent rainfall anomalies, for example, have greatly reduced crop productivity in the Sahel area. Rainfall indices from recent centuries show that multidecadal droughts reoccur and, furthermore, that interannual rainfall variations are high in West Africa. Current knowledge of historical rainfall patterns is, however, fairly limited. A detailed rainfall chronology of West Africa is currently only available from the beginning of the 19th century. For the

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25

Hameed, Saji N. The Indian Ocean Dipole. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.619.

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Discovered at the very end of the 20th century, the Indian Ocean Dipole (IOD) is a mode of natural climate variability that arises out of coupled ocean–atmosphere interaction in the Indian Ocean. It is associated with some of the largest changes of ocean–atmosphere state over the equatorial Indian Ocean on interannual time scales. IOD variability is prominent during the boreal summer and fall seasons, with its maximum intensity developing at the end of the boreal-fall season. Between the peaks of its negative and positive phases, IOD manifests a markedly zonal see-saw in anomalous sea surface

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26

Goswami, B. N., and Soumi Chakravorty. Dynamics of the Indian Summer Monsoon Climate. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.613.

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Lifeline for about one-sixth of the world’s population in the subcontinent, the Indian summer monsoon (ISM) is an integral part of the annual cycle of the winds (reversal of winds with seasons), coupled with a strong annual cycle of precipitation (wet summer and dry winter). For over a century, high socioeconomic impacts of ISM rainfall (ISMR) in the region have driven scientists to attempt to predict the year-to-year variations of ISM rainfall. A remarkably stable phenomenon, making its appearance every year without fail, the ISM climate exhibits a rather small year-to-year variation (the sta

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27

Lachniet, Matthew S., and Juan Pablo Bernal-Uruchurtu. AD 550–600 Collapse at Teotihuacan. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780199329199.003.0006.

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We analyze a 2400-year rainfall reconstruction from an ultra-high-resolution absolutely-dated stalagmite (JX-6) from southwestern Mexico (Lachniet et al., 2012). Oxygen isotope variations correlate strongly to rainfall amount in the Mexico City area since 1870 CE, and for the wider southwestern Mexico region since 1948, allowing us to quantitatively reconstruct rainfall variability for the Basin of Mexico and Sierra Madre del Sur for the past 2400 years. Because oxygen isotopes integrate rainfall variations over broad geographic regions, our data suggest substantial variations in Mesoamerican

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28

Robin, Libby, Robert Heinsohn, and Leo Joseph, eds. Boom and Bust. CSIRO Publishing, 2009. http://dx.doi.org/10.1071/9780643097094.

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In Boom and Bust, the authors draw on the natural history of Australia's charismatic birds to explore the relations between fauna, people and environment in a continent where variability is 'normal' and rainfall patterns not always seasonal. They consider changing ideas about deserts and how these have helped us understand birds and their behaviour in this driest of continents. The book describes the responses of animals and plants to environmental variability and stress. It is also a cultural concept, when it is used to capture the patterns of change wrought by humans in Australia, wher

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Newman, Chris, Christina D. Buesching, and David W. Macdonald. Meline mastery of meteorological mayhem: the effects of climate changeability on European badger population dynamics. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198759805.003.0021.

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Adaptation to climatic conditions is a major ecological and evolutionary driver. Long-term study of European badger population dynamics in Oxfordshire reveals that rainfall and temperature patterns affect food (principally earthworm) availability, energy expended in thermoregulation, and activity patterns, with badgers able to seek refuge in their setts. Cubs prove especially vulnerable to harsh weather conditions, where drought and food shortages exacerbate the severity of pandemic juvenile coccidial parasite infections. Crucially, weather variability, rather than just warming trends, stresse

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30

Mbow, Cheikh. The Great Green Wall in the Sahel. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.559.

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For several decades, the Sahelian countries have been facing continuing rainfall shortages, which, coupled with anthropogenic factors, have severely disrupted the great ecological balance, leading the area in an inexorable process of desertification and land degradation. The Sahel faces a persistent problem of climate change with high rainfall variability and frequent droughts, and this is one of the major drivers of population’s vulnerability in the region. Communities struggle against severe land degradation processes and live in an unprecedented loss of productivity that hampers their livel

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31

Wangui, Edna. Adaptation to Current and Future Climate in Pastoral Communities Across Africa. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.604.

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Pastoralists around the world are exposed to climate change and increasing climate variability. Various downscaled regional climate models in Africa support community reports of rising temperatures as well as changes in the seasonality of rainfall and drought. In addition to climate, pastoralists have faced a second exposure to unsupportive policy environments. Dating back to the colonial period, a lack of knowledge about pastoralism and a systemic marginalization of pastoral communities influenced the size and nature of government investments in pastoral lands. National governments prioritize

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32

Fensholt, Rasmus, Cheikh Mbow, Martin Brandt, and Kjeld Rasmussen. Desertification and Re-Greening of the Sahel. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.553.

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In the past 50 years, human activities and climatic variability have caused major environmental changes in the semi-arid Sahelian zone and desertification/degradation of arable lands is of major concern for livelihoods and food security. In the wake of the Sahel droughts in the early 1970s and 1980s, the UN focused on the problem of desertification by organizing the UN Conference on Desertification (UNCOD) in Nairobi in 1976. This fuelled a significant increase in the often alarmist popular accounts of desertification as well as scientific efforts in providing an understanding of the mechanism

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